海洋科学进展
海洋科學進展
해양과학진전
JOURNAL OF OCEANOGRAPHY OF HUANGHAI & BOHAI SEAS
2015年
2期
131-141
,共11页
吴伦宇%郑斌鑫%曾志%何佳%陈志杰
吳倫宇%鄭斌鑫%曾誌%何佳%陳誌傑
오륜우%정빈흠%증지%하가%진지걸
粤东%甲子海域%潮流%潮流谱分析
粵東%甲子海域%潮流%潮流譜分析
월동%갑자해역%조류%조류보분석
East Guangdong%waters adjacent to Jiazi%tidal current%tidal current spectrum analysis
针对2012‐04—07甲子以东海域3个站的潮位和海流连续观测资料,采用潮汐和潮流调和分析、海流旋转功率谱等方法,研究了它们的潮汐和各层潮流的分布特征,探讨了这些特征形成的原因。结果表明:1)甲子港及其以东40 km海域典型日潮的形成是由于M2分潮的无潮点的存在和潮能在甲子外海的辐散两种原因引起的;2)日潮海域的潮流则是正规半日潮流的性质;3)研究海域的潮波较为复杂,驻波性质不明显,前进波性质较为突出;4)通过类比黄河口M2分潮的无潮点,认为该海区存在一个退化到岸上的M2无潮点是可能的。
針對2012‐04—07甲子以東海域3箇站的潮位和海流連續觀測資料,採用潮汐和潮流調和分析、海流鏇轉功率譜等方法,研究瞭它們的潮汐和各層潮流的分佈特徵,探討瞭這些特徵形成的原因。結果錶明:1)甲子港及其以東40 km海域典型日潮的形成是由于M2分潮的無潮點的存在和潮能在甲子外海的輻散兩種原因引起的;2)日潮海域的潮流則是正規半日潮流的性質;3)研究海域的潮波較為複雜,駐波性質不明顯,前進波性質較為突齣;4)通過類比黃河口M2分潮的無潮點,認為該海區存在一箇退化到岸上的M2無潮點是可能的。
침대2012‐04—07갑자이동해역3개참적조위화해류련속관측자료,채용조석화조류조화분석、해류선전공솔보등방법,연구료타문적조석화각층조류적분포특정,탐토료저사특정형성적원인。결과표명:1)갑자항급기이동40 km해역전형일조적형성시유우M2분조적무조점적존재화조능재갑자외해적복산량충원인인기적;2)일조해역적조류칙시정규반일조류적성질;3)연구해역적조파교위복잡,주파성질불명현,전진파성질교위돌출;4)통과류비황하구M2분조적무조점,인위해해구존재일개퇴화도안상적M2무조점시가능적。
T he characteristics of the tide and the tidal current at three stations to the east of Jiazi are studied based on measurments from April to July ,2004 and methods of harmonic analysis and rotary spectrum . Results show that :1) The typical diurnal tide formed at Jiazi port and its east waters is due to the ex‐sitence of M2 tidal amphidromic point and the divergence of the tidal energy in the waters off Jiazi ;2) Al‐though the tide is dirnal ,the tidal current is regular semidiurnal ;3)Tidal wave in the concerned area is rel‐atively complicated where the characteristic of progressive wave properties is more obvious than that of standing wave;4)In analogy with the M2 tidal amphidromic point in Yellow River mouth ,a M2 tidal am‐phidromic point degenerated on land is considered possible there .